Holocene Rice Rats (Genus Oryzomys) from the Upper Mississippi River Drainage Basin

Zea Books Pub Date : 2023-08-15 DOI:10.32873/unl.dc.zea.1502
Hugh Genoways
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Abstract

The expansion and collapse of the geographic range of the Texas rice rat (Oryzomys texensis) in the upper Mississippi River drainage basin at the end of the Holocene was a unique event in North American mammals. In a period of about 4000 years with a point of origin near the American Bottom in Illinois, these small rodents extended their geographic range in a straight-line distance of over 950 km to the west into Nebraska and the same distance to the east into Pennsylvania. Then in less than 400 years this range expansion collapsed back to a point where the northern-most edge of the modern geographic range of these rice rats is in southern Illinois. It is concluded that no single factor lead to this geographic range expansion, but it was a complex interplay of changes in Native American populations, culture, foodways, riverine habitats, and climate along with the impact of kleptoparasitism and passive anthropochory. The collapse of the expanded geographic range of Texas rice rats appears to have occurred between AD 1400 and AD 1600, but it did not occur simultaneously throughout the geographic range. This was not an orderly range contraction, but a collapse of populations in place with many local extinction events. These rice rat populations declined beginning with the onset of the Little Ice Age, which brought a colder and wetter climate that caused crop failures resulting from droughts, cold temperatures, or shortened growing seasons. These conditions stressed the dietary reserves of the human populations and thereby the rice rat populations. These conditions, particularly droughts, were harmful to the growing of maize, which served as the primary food resource of the Native Americans and the associated populations of rice rats. It is proposed that the pre-1910 records of rice rat from unusual localities compared to the modern geographic range in southwestern Ohio, Kentucky, and Kansas represent the final extinction events of these Holocene rice rat populations.
密西西比河上游流域全新世稻鼠(稻鼠属)
全新世末期,得克萨斯稻鼠(Oryzomys texensis)在密西西比河流域上游地理范围的扩张和缩小是北美哺乳动物中一个独特的事件。在大约4000年的时间里,这些小型啮齿类动物以美国伊利诺斯州的海底附近为起点,将它们的地理范围直线扩展了950多公里,向西延伸到内布拉斯加州,向东延伸到宾夕法尼亚州。然后,在不到400年的时间里,这种范围的扩张又回到了一个点,在那里,这些稻鼠现代地理范围的最北端位于伊利诺伊州南部。结论是,没有单一因素导致这种地理范围的扩大,而是美洲原住民人口、文化、食物方式、河流栖息地和气候变化以及盗窃寄生和被动人类学的影响的复杂相互作用。德克萨斯稻鼠扩大的地理范围的崩溃似乎发生在公元1400年至1600年之间,但它并不是同时发生在整个地理范围内。这不是一个有序的范围收缩,而是种群的崩溃,伴随着许多局部灭绝事件。这些稻鼠的数量从小冰期开始下降,小冰期带来了更冷更湿的气候,导致干旱、低温或生长季节缩短导致作物歉收。这些条件强调了人类种群的饮食储备,从而强调了稻鼠种群。这些条件,尤其是干旱,对玉米的生长是有害的,玉米是美洲原住民和相关稻鼠群体的主要食物来源。作者认为,1910年以前在俄亥俄、肯塔基和堪萨斯州西南部的不同地理范围的稻鼠记录代表了这些全新世稻鼠种群的最终灭绝事件。
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